Ash and Tephra Hazards from Yellowstone

The most likely type of volcanic eruption at Yellowstone would produce lava flows of either
rhyolite or basalt; rhyolitic lava eruptions could also include explosive phases that might produce
significant volumes of volcanic ash and pumice. Such eruptions could range in size from smaller than
the 1980 eruption of Mt. St. Helens through much larger than the 1991 Mount Pinatubo eruption.

The least likely but worst-case volcanic eruption at Yellowstone would be another explosive caldera-
forming eruption such as those that occurred 2.1 million, 1.3 million, and 640,000 years ago. Such
an eruption would produce ash columns that exceed 10 km (6 mi) and cover much of the United
States with some ash. Once entering the stratosphere (higher than about 10 km or 6 mi), the ash
particles would circle the globe and, in combination with the sulfur dioxide emitted during an
eruption, could cause global temperatures to drop. However, the probability of such an eruption in
any given century or millennium is exceedingly low — much lower than a hydrothermal
explosion or lava flow
eruption.